Slope Stability and Mass Movement

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Flashcards to help study the key terms and concepts related to slope stability and mass movement.

Last updated 10:52 PM on 6/4/25
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25 Terms

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Slope

A sloped surface on the landscape, which can be rock slopes or soil-covered slopes. (Crozier, 1986)

<p>A sloped surface on the landscape, which can be rock slopes or soil-covered slopes. (Crozier, 1986)</p><ul><li><p></p><img src="https://knowt-user-attachments.s3.amazonaws.com/f6fbb083-0983-43b0-b36a-a5f911c4388c.png" data-width="100%" data-align="center"></li></ul><p></p>
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Mass movement

The movement of soil and rock material down a slope due to gravity. (Crozier, 1986) - catastrophic

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Shear stress

The stress component that acts parallel to the surface of a material. (Crozier, 1986)

slope falls because of stress or strength

<p>The stress component that acts parallel to the surface of a material. (Crozier, 1986)</p><p>slope falls because of stress or strength </p>
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Shear strength

The internal resistance of a material to shear stress, determined by effective normal stress and cohesion. (Crozier, 1986)

<p>The internal resistance of a material to shear stress, determined by effective normal stress and cohesion. (Crozier, 1986)</p><p></p>
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Landslide

A sudden and fast movement of a large amount of earth material down a slope. (Crozier, 1986)

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Triggers of landslides

Factors such as heavy rainfall, earthquakes, or human activities that can initiate a landslide. (Crozier, 1986)

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Tectonic activity

Geological processes associated with the movement of the Earth's lithosphere, often associated with landslides in active regions.

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Creep

The slow, gradual movement of soil or rock down a slope. (Crozier, 1986)

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Pore pressure

Pressure exerted by water within the pores of soil or rock, affecting slope stability. (Crozier, 1986)

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Coulomb-Terzaghi equation

An equation used to calculate shear strength of a slope based on normal stress and cohesion. (Crozier, 1986)

<p>An equation used to calculate shear strength of a slope based on normal stress and cohesion. (Crozier, 1986)</p><p></p>
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Effects of gravity on slopes

Gravity pushing down on an object

when balance changes between forces - land moves

<p>Gravity pushing down on an object </p><p>when balance changes between forces - land moves </p>
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Stable slope

Normal force is greater than shear stress

<p>Normal force is greater than shear stress </p>
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Conditionally unstable slope

Normal force is equal to or greater than shear stress

<p>Normal force is equal to or greater than shear stress </p>
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Actively unstable slope

slope is failing

threshold provides a set of conditions

<p>slope is failing </p><p>threshold provides a set of conditions </p>
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Water content

particles stick together

more water - slope falls more quickly

<p>particles stick together </p><p>more water - slope falls more quickly </p>
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Slope materials and structure

  • (Kirkby, 2005)

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application to geomorphological hazards

 

<p>&nbsp;</p><img src="https://knowt-user-attachments.s3.amazonaws.com/cfb4b33a-4fad-4a58-9499-1bfa86107dfb.png" data-width="100%" data-align="center"><p></p>
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Measuring shear stress

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Factors affecting slope stability

(Kirkby, 2005)

<p>(Kirkby, 2005)</p>
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Factors to consider

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Preparatory factors and triggers

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Continued

<ul><li><p></p><img src="https://knowt-user-attachments.s3.amazonaws.com/9254a4e1-7e43-4c2d-a05f-f4c062ca4c31.png" data-width="100%" data-align="center"></li></ul><p></p>
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Case study: North Norfolk Coast

 

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Geographic clues to mass movement

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Case study: Nepal